https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html

Local temperature response to land cover and management change driven by
non-radiative processes

   - Ryan M. Bright
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#auth-1>,

   - Edouard Davin
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#auth-2>,

   - Thomas O’Halloran
   <https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#auth-3>
   ,
   - Julia Pongratz
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#auth-4>,

   - Kaiguang Zhao
   <https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#auth-5>
   - & Alessandro Cescatti
   <https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#auth-6>


   - Affiliations
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#affil-auth>
   - Contributions
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#contrib-auth>
   - Corresponding author
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#corres-auth>

Nature Climate Change 7, 296–302 (2017)doi:10.1038/nclimate3250Received 18
July 2016 Accepted 21 February 2017Published online 27 March 2017
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Abstract

   - Abstract•
   - References
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#references>
   •
   - Author information
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#author-information>
   •
   - Supplementary information
   
<https://www.nature.com/nclimate/journal/v7/n4/full/nclimate3250.html#supplementary-information>

Following a land cover and land management change (LCMC), local surface
temperature responds to both a change in available energy and a change in
the way energy is redistributed by various non-radiative mechanisms.
However, the extent to which non-radiative mechanisms contribute to the
local direct temperature response for different types of LCMC across the
world remains uncertain. Here, we combine extensive records of remote
sensing and *in situ* observation to show that non-radiative mechanisms
dominate the local response in most regions for eight of nine common LCMC
perturbations. We find that forest cover gains lead to an annual cooling in
all regions south of the upper conterminous United States, northern Europe,
and Siberia—reinforcing the attractiveness of re-/afforestation as a local
mitigation and adaptation measure in these regions. Our results affirm the
importance of accounting for non-radiative mechanisms when evaluating local
land-based mitigation or adaptation policies.
Subject terms:

   - Climate and Earth system modelling
   <https://www.nature.com/subjects/climate-and-earth-system-modelling>
   - Climate-change mitigation
   <https://www.nature.com/subjects/climate-change-mitigation>

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